FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2168613637> ?p ?o ?g. }

• W2168613637 endingPage "3326" @default.
• W2168613637 startingPage "3303" @default.
• W2168613637 abstract "Abstract. The present study investigates the radiative effects of dust aerosols in the Mediterranean region during summer 2012 using a coupled regional aerosol–atmosphere–ocean model (CNRM-RCSM5). A prognostic aerosol scheme, including desert dust, sea salt, organic, black-carbon and sulphate particles, has been integrated to CNRM-RCSM5 in addition to the atmosphere, land surface and ocean components. An evaluation of this aerosol scheme of CNRM-RCSM5, and especially of the dust aerosols, has been performed against in situ and satellite measurements, showing its ability to reproduce the spatial and temporal variability of aerosol optical depth (AOD) over the Mediterranean region in summer 2012. The dust vertical and size distributions have also been evaluated against observations from the TRAQA/ChArMEx campaign. Three simulations have been carried out for summer 2012 with CNRM-RCSM5, including the full prognostic aerosol scheme, only monthly-averaged AOD means from the aerosol scheme or no aerosols at all, in order to focus on the radiative effects of dust particles and the role of the prognostic scheme. Surface short-wave aerosol radiative forcing variability is found to be more than twice as high over regions affected by dust aerosols, when using a prognostic aerosol scheme instead of monthly AOD means. In this case downward surface solar radiation is also found to be better reproduced according to a comparison with several stations across the Mediterranean. A composite study over 14 stations across the Mediterranean, designed to identify days with high dust AOD, also reveals the improvement of the representation of surface temperature brought by the use of the prognostic aerosol scheme. Indeed the surface receives less radiation during dusty days, but only the simulation using the prognostic aerosol scheme is found to reproduce the observed intensity of the dimming and warming on dusty days. Moreover, the radiation and temperature averages over summer 2012 are also modified by the use of prognostic aerosols, mainly because of the differences brought in short-wave aerosol radiative forcing variability. Therefore this first comparison over summer 2012 highlights the importance of the choice of the representation of aerosols in climate models." @default.
• W2168613637 created "2016-06-24" @default.
• W2168613637 creator A5003319020 @default.
• W2168613637 creator A5007474312 @default.
• W2168613637 creator A5009896242 @default.
• W2168613637 creator A5011294624 @default.
• W2168613637 creator A5040346477 @default.
• W2168613637 creator A5044638940 @default.
• W2168613637 creator A5045857325 @default.
• W2168613637 creator A5049948880 @default.
• W2168613637 creator A5059635034 @default.
• W2168613637 creator A5059764363 @default.
• W2168613637 creator A5061451910 @default.
• W2168613637 creator A5077272435 @default.
• W2168613637 creator A5079047247 @default.
• W2168613637 date "2015-03-24" @default.
• W2168613637 modified "2023-10-02" @default.
• W2168613637 title "Dust aerosol radiative effects during summer 2012 simulated with a coupled regional aerosol–atmosphere–ocean model over the Mediterranean" @default.
• W2168613637 cites W1249428219 @default.
• W2168613637 cites W1834577838 @default.
• W2168613637 cites W1963839881 @default.
• W2168613637 cites W1965151843 @default.
• W2168613637 cites W1970047006 @default.
• W2168613637 cites W1970212020 @default.
• W2168613637 cites W1971398176 @default.
• W2168613637 cites W1974342476 @default.
• W2168613637 cites W1980583318 @default.
• W2168613637 cites W1981126864 @default.
• W2168613637 cites W1983073756 @default.
• W2168613637 cites W1985109297 @default.
• W2168613637 cites W1985479415 @default.
• W2168613637 cites W1985582255 @default.
• W2168613637 cites W1985613397 @default.
• W2168613637 cites W1987461785 @default.
• W2168613637 cites W1988509955 @default.
• W2168613637 cites W1999979375 @default.
• W2168613637 cites W2000436415 @default.
• W2168613637 cites W2002486217 @default.
• W2168613637 cites W2012247153 @default.
• W2168613637 cites W2014670354 @default.
• W2168613637 cites W2015071544 @default.
• W2168613637 cites W2018958057 @default.
• W2168613637 cites W2019976017 @default.
• W2168613637 cites W2033499347 @default.
• W2168613637 cites W2039363399 @default.
• W2168613637 cites W2040422439 @default.
• W2168613637 cites W2040746851 @default.
• W2168613637 cites W2048512417 @default.
• W2168613637 cites W2050161743 @default.
• W2168613637 cites W2054903488 @default.
• W2168613637 cites W2056283761 @default.
• W2168613637 cites W2058759684 @default.
• W2168613637 cites W2065444076 @default.
• W2168613637 cites W2067486888 @default.
• W2168613637 cites W2067726355 @default.
• W2168613637 cites W2068735446 @default.
• W2168613637 cites W2078517784 @default.
• W2168613637 cites W2079827920 @default.
• W2168613637 cites W2083339292 @default.
• W2168613637 cites W2086145959 @default.
• W2168613637 cites W2089433206 @default.
• W2168613637 cites W2092758993 @default.
• W2168613637 cites W2093234629 @default.
• W2168613637 cites W2094408786 @default.
• W2168613637 cites W2106963750 @default.
• W2168613637 cites W2112335693 @default.
• W2168613637 cites W2113973563 @default.
• W2168613637 cites W2115955657 @default.
• W2168613637 cites W2117901674 @default.
• W2168613637 cites W2121745948 @default.
• W2168613637 cites W2123293242 @default.
• W2168613637 cites W2130578813 @default.
• W2168613637 cites W2136449662 @default.
• W2168613637 cites W2137274987 @default.
• W2168613637 cites W2139273826 @default.
• W2168613637 cites W2139452943 @default.
• W2168613637 cites W2139836399 @default.
• W2168613637 cites W2139937607 @default.
• W2168613637 cites W2140397818 @default.
• W2168613637 cites W2142306678 @default.
• W2168613637 cites W2145446721 @default.
• W2168613637 cites W2145943926 @default.
• W2168613637 cites W2148807170 @default.
• W2168613637 cites W2152311585 @default.
• W2168613637 cites W2153306945 @default.
• W2168613637 cites W2153438006 @default.
• W2168613637 cites W2171368857 @default.
• W2168613637 cites W2319391253 @default.
• W2168613637 cites W2320145997 @default.
• W2168613637 cites W2321587562 @default.
• W2168613637 cites W2626335618 @default.
• W2168613637 cites W4234843088 @default.
• W2168613637 cites W92888908 @default.
• W2168613637 doi "https://doi.org/10.5194/acp-15-3303-2015" @default.
• W2168613637 hasPublicationYear "2015" @default.
• W2168613637 type Work @default.
• W2168613637 sameAs 2168613637 @default.
• W2168613637 citedByCount "82" @default.

• next